Biogeographical assessment of · 2017-07-18 · Journal of Biogeography 44, 1524–1536 ª 2017...
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ORIGINALARTICLE
Biogeographical assessment ofmyxomycete assemblages fromNeotropical and Asian PalaeotropicalforestsNikki Heherson A. Dagamac1* , Yuri K. Novozhilov2,3,
Steven L. Stephenson4, Carlos Lado5, Carlos Rojas6,
Thomas Edison E. dela Cruz7, Martin Unterseher1 and Martin Schnittler1
1Institute of Botany and Landscape Ecology,
Ernst Moritz Arndt University Greifswald,
Soldmannstr. 15, D-17487 Greifswald,
Germany, 2Laboratory of Systematics and
Geography of Fungi, Komarov Botanical
Institute of the Russian Academy of Sciences,
Prof. Popov Street 2, 197376 St. Petersburg,
Russia, 3Joint Russian-Vietnamese Tropical
Research and Technological Centre of the
A.N. Severtsov Institute of Ecology and
Evolution RAS, South Branch 3, Street 3/2,
10 District, Ho Chi Minh City, Vietnam,4Department of Biological Sciences, University
of Arkansas, Fayetteville, AR 72701, USA,5Real Jard�ın Bot�anico, CSIC, Plaza de
Murillo 2, 28014 Madrid, Spain, 6Engineering
Research Institute and Department of
Agricultural Engineering, University of Costa
Rica, San Pedro de Montes de Oca 11501,
Costa Rica, 7Department of Biological
Sciences, University of Santo Tomas, Espa~na,
1015 Manila, Philippines
*Correspondence: Nikki Heherson A.
Dagamac, Institute of Botany and Landscape
Ecology, Ernst Moritz Arndt University
Greifswald, Soldmannstr. 15, D-17487
Greifswald, Germany.
E-mail: [email protected]
ABSTRACT
Aim Lowland/highland and Neotropical/Asian Palaeotropical assemblages of
myxomycetes were compared to test the null hypothesis that neither species
diversity nor species composition differs between the two ecoregions. This can
be expected if myxomycetes behave as ubiquists and are capable of unlimited
long distance dispersal.
Location Four pairs (lowland/highland) of comprehensive regional surveys
encompassing c. 7500 specimens were compared; these represented Neotropical
(Yasuni/Maquipucuna in Ecuador; Guanacaste/Monteverde in Costa Rica) and
Asian Palaeotropical forests (Cat Tien/Bi Dup Nui Ba in Vietnam; Chiang Mai
in Thailand/South Luzon in the Philippines).
Methods Each survey was carried out in an area characterized by relatively
homogenous vegetation consisting of natural or near-natural forests, and incor-
porated both field collecting and the use of moist chamber cultures, and all
observed fructifications were recorded. Analyses of diversity (i.e. richness) and
community composition were carried out with EstimateS and R.
Results Between 400 and 2500 records per survey were obtained. Species accu-
mulation curves indicated moderate to nearly exhaustive completeness (70–94% of expected species richness recorded). Multivariate analyses suggest that
geographical separation (Neotropic versus Palaeotropic) explained the observed
differences in composition of myxomycete assemblages better than habitat
differences (lowland versus highland forests).
Main Conclusion Both geographically restricted morphospecies and differ-
ences in myxomycete assemblages provide evidence that myxomycetes are not
ubiquists but tend to follow the moderate endemicity hypothesis of protist
biogeography.
Keywords
Amoebozoa, community ecology, dispersal barriers, endemicity, morphos-
pecies, myxomycete, plasmodial slime moulds
INTRODUCTION
Myxomycetes (plasmodial slime moulds) are one of the few
protist groups that can be studied in the field, based on their
above-ground macroscopic fructifications which release air-
borne spores (Schnittler et al., 2012). Most of our knowledge
about myxomycete assemblages has been derived from sur-
veys which have recorded fructifications in the field or from
moist chamber cultures (Stephenson et al., 2008). In terms
of biogeography, most studies have been carried out in tem-
perate regions of the Northern Hemisphere, including alpine
and subalpine mountains (Ronikier & Ronikier, 2009;
Novozhilov et al., 2013), tundra (Novozhilov et al., 1999;
Stephenson et al., 2000), winter-cold deserts (Schnittler &
Novozhilov, 2000; Schnittler, 2001; Novozhilov & Schnittler,
2008) and temperate grasslands (Rollins & Stephenson,
2013). Only recently have other parts of the world, such as
tropical zones, warm deserts or the Patagonian steppe been
1524 http://wileyonlinelibrary.com/journal/jbi ª 2017 John Wiley & Sons Ltddoi:10.1111/jbi.12985
Journal of Biogeography (J. Biogeogr.) (2017) 44, 1524–1536
studied systematically (Estrada-Torres et al., 2009; Wrigley
de Basanta et al., 2010; Lado et al., 2013, 2014, 2016). At the
level of morphologically recognizable taxa, many myx-
omycete species display cross-continental distribution pat-
terns (Stephenson et al., 2008). Even remote islands such as
the Galapagos Islands (Eliasson & Nannenga-Bremekamp,
1983), the Hawaiian archipelago (Eliasson, 1991), Macquarie
Island (Stephenson et al., 2007) or Bohol Island (Macabago
et al., 2017) do not seem to have endemic taxa present.
In contrast, numerous myxomycete species described
within the last few decades (Schnittler & Mitchell, 2000) are
known from only one or a few localities. Moreover, certain
vegetation types contain species that are locally abundant but
do not occur elsewhere. This is best documented for deserts;
examples include Physarum pseudonotabile Novozh., Schnit-
tler & Okun in Central Asia (Novozhilov & Schnittler, 2008;
Novozhilov et al., 2013), or Perichaena calongei Lado, D.
Wrigley & Estrada, Didymium infundibuliforme D. Wrigley,
Lado & Estrada and Physarum atacamense D. Wrigley, Lado
& Estrada in South America (Lado et al., 2009; Wrigley de
Basanta et al., 2009, 2012; Araujo et al., 2015). Whether this
is due to the lack of data from many areas of the world or
due to some morphologically recognizable myxomycete spe-
cies occurring with a limited distribution is a question being
debated. In spite of their capability for long distance disper-
sal via spores (Kamono et al., 2009), it seems that in keeping
with other eukaryotic protists such as testate amoebae, cili-
ates and diatoms (Foissner, 2006, 2008), myxomycetes may
support the moderate endemicity hypothesis (Foissner, 1999)
for protist biogeography. This hypothesis recognizes that cos-
mopolitan species of protists may exist in nature but due to
geographical barriers, about 30% of all species can show geo-
graphically restricted distributions.
Various studies have reported species of myxomycetes
fruiting predominantly in specific vegetation types (Schnittler
& Stephenson, 2000), on particular substrates (Wrigley de
Basanta et al., 2008; Tucker et al., 2011), or during certain
seasons (Rojas & Stephenson, 2007; Dagamac et al., 2012).
The unresolved question is whether such differences are
entirely the result of microhabitat preferences (wherever suit-
able substrata occur under suitable microclimatic conditions,
the respective species will fruit), as suggested for Barbeyella
minutissima Meyl. (Schnittler et al., 2000). If microhabitat
suitability represents the only factor determining occurrence,
effective long-distance dispersal or persistent populations of
amoebae must be assumed. Indeed, 18S rRNA gene
sequences of the commonly highland fruiting nivicolous
genus Meriderma were already detected in lowland regions,
indicating persistence (presumably of amoebae) where this
taxon never fruits (Fiore-Donno et al., 2016). Furthermore,
another explanation is to assume the existence of barriers to
distribution, at least between continents (Estrada-Torres
et al., 2013; Aguilar et al., 2014). Long-distance dispersal has
been reported for myxomycetes (Kamono et al., 2009), and
the patchy occurrence of nivicolous myxomycetes in moun-
tain ranges of the Northern and Southern Hemispheres
corroborates this (Ronikier & Lado, 2015). Thus, transconti-
nental dispersal events may happen, but it is unknown if the
frequency of gene flow mediated by spore dispersal is suffi-
cient to prevent allopatric speciation from occurring between
transcontinental populations. As has been shown for the
much better documented ferns and fern allies (usually pos-
sessing much larger spores), species may show transcontinen-
tal distribution patterns or may be restricted to one
continent only (Karst et al., 2005).
An adequate ‘field laboratory’ to address the question of
myxomycetes distribution would be a major ecosystem that
is stable for a long period of time and is globally distributed
– in other words, tropical regions covered naturally by rain
forests. For myxomycetes, many diversity assessments have
been carried out in Neotropical forests. These range from
country checklists (Brazil, Cavalcanti, 2010; Colombia, Rojas
et al., 2012a; Costa Rica, Rojas et al., 2010; El Salvador,
Rojas et al., 2013) to abundance-based diversity assessments
of natural habitats (Lado et al., 2003; Rojas & Stephenson,
2012). About half of the c. 1000 known morphospecies of
myxomycetes (Lado, 2005–2016) have been recorded from
the Neotropics (Lado & Wrigley de Basanta, 2008). Our
knowledge of myxomycete diversity of the Asian Palaeotrop-
ics is more limited, and c. 200 taxa are known. Nevertheless,
several investigations have been carried out in lowland and
montane vegetation types of Southeast Asia, including Thai-
land (Tran et al., 2008; KoKo et al., 2010), Singapore (Ros-
ing et al., 2011), Laos (KoKo et al., 2012), Vietnam
(Novozhilov & Mitchell, 2014; Novozhilov et al., 2014; Tran
et al., 2014; Novozhilov & Stephenson, 2015) and the Philip-
pines (Dagamac et al., 2015a,b, 2017).
This study compared myxomycete assemblages between
Neotropical and Asian Palaeotropical forests with the objec-
tive of answering several questions: First, are there differences
in species composition and/or species abundance between
(1) different vegetation types within a particular region
(tropical lowland versus highland forests) or (2) comparable
vegetation types on different continents (Asian Palaeotropics:
Thailand, Philippines and Vietnam versus Neotropics: Costa
Rica and Ecuador)? Second, are there species apparently
restricted to only one of the regions in question? Third, does
a comparison of regional survey data provide evidence to
support the ‘moderate endemicity’ hypothesis (Foissner,
2006) for eukaryotic protists?
MATERIALS AND METHODS
Compilation of regional datasets
A double-paired design (four Neotropical and four Asian
Palaeotropical/four lowland and four highland areas, Fig. 1,
Table 1) was chosen to identify differences in species compo-
sition and abundance associated with geography and/or ele-
vation as a proxy for habitat type. Five criteria were applied
to select the eight datasets used in this study. (1) The area
for each survey should be relatively homogenous for a major
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forest type. (2) The two components of a survey should
include at least 100 records from the field collections plus
100 records obtained by the moist chamber culture tech-
nique, with all major substrata (bark, aerial and ground lit-
ter) roughly equally represented. (3) Records should include
all fructifications observed in the field or in cultures, which
may be determined on the spot or collected for later deter-
mination. This allowed abundance estimates to be compiled
for all of the species present, but excluded many published
studies which provided only pure species lists without abun-
dance data. (4) The exhaustiveness of a survey should exceed
70% in order to recover the majority of species likely to
occur in a particular region. In a strict sense, this could not
be verified. As a proxy criterion, we checked if the Chao1
estimator for an individual-based accumulation curve (in-
cluding all records from each survey) converged (standard
deviation should not monotonously increase but decrease
with increasing number of records) and if its final value
Figure 1 World map showing the eight areas surveyed for myxomycetes that were used in this study, the number of records found andthe total number of species accounted on each survey. [Colour figure can be viewed at wileyonlinelibrary.com]
Table 1 Characteristics of the eight investigated areas in the Neotropical and Asian Palaeotropics; naming the investigated area,
literature references, elevation and geographical coordinates, the number of moist chamber cultures prepared and vegetation types,applying by Holdridge et al. (1971) classification of tropical forests. Surveys are listed in the sequence Neotropical/Palaeotropical (N/P)
and lowland/highland (L/H) for each region.
Region Reference
Elevation
(m a.s.l.) Location
Moist chamber
cultures Vegetation type
NL: Costa Rica,
Guanacaste
Schnittler & Stephenson
(2000)
10–300 08°470–10°580 N82°490–85°560 W
476 Tropical dry forest (excluding
volcano Cacao)
NL: Ecuador,
Yasuni
Lado et al. (2017) 200–275 04°000–04°040 N76°220–76°250 W
225 Tropical moist forest, Amazonian
lowland forest
NH: Costa Rica,
Monteverde
Rojas et al. (2010) 1000–1500 10°160–10°190 N84°440–84°480 W
c. 700 Tropical montane wet forest
NH: Ecuador,
Maquipucuna
Schnittler et al. (2002),
Stephenson et al. (2004a)
1250–2720 03°150–07°280 N78°340–78°280 W
475 Tropical montane wet forest
PL: Philippines,
South Luzon
Dagamac et al. (2017, 2015b) 10–524 12°750–14°100 0N120°540–124°090 E
1500 Tropical moist forest
PL: Vietnam, Cat
Tien
Novozhilov et al. (2017) 72–247 11°160–11°270 N107°030–107°260 E
954 Tropical moist forest
PH: Thailand,
Chiang Mai
Dagamac, N.H.A., Unterseher, M. &
Schnittler, M., unpublished
data; Rojas et al. (2012b),
KoKo et al. (2010);
900–2500 18°480–20°100 N98°290–99°720 E
c. 1000 Tropical montane wet forest
PH: Vietnam, Bi
Dup Nui Ba
Novozhilov, personal
communication
1375–1747 12°070–12°110 N108°380–108°420 E
922 Tropical montane wet forest
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N. H. A. Dagamac et al.
indicated a completeness of at least 70% (ratio observed to
expected species). (5) The habitats studied within a survey
should include at least pockets of natural or near-natural for-
ests, to reflect the natural species inventory to a significant
degree.
Moist chamber cultures and specimen determination
Moist chamber cultures were prepared in 9 cm Petri dishes
using standard procedures (e.g. Schnittler, 2001), incubated
under ambient light at room temperature (c. 20–24 °C) for
up to 90 days and checked regularly on at least five occa-
sions. To maintain moisture, distilled water was added over
the first 6 weeks of the incubation period. Mature fructifica-
tions were transferred to herbarium boxes, with one record
defined as a colony of fructifications from a single taxon
developing in one culture. Myxomycete taxa were deter-
mined according to morphological characters of the fructifi-
cations, using standard monographs of the group (e.g.
Nannenga-Bremekamp, 1967, 1991; Martin & Alexopoulos,
1969; Farr, 1976; Neubert et al., 1995–2000; Lado & Pando,
1997; Poulain et al., 2011) and public repositories (Eumyce-
tozoan Project at http://slimemold.uark.edu/; Discover Life at
http://www.discoverlife.org). Nomenclature follows Lado
(2005–2016). Voucher specimens are deposited in the
herbarium of the University of Arkansas (UARK), the Botan-
ical State Collection Munich (M), the herbarium of the
University of Costa Rica at San Jose (USJ), the Real Jard�ın
Bot�anico de Madrid, (MA-fungi), the University of Santo
Tomas, Manila (USTH) and the Komarov Botanical Institute
(LE).
Data analysis
Individual-based species accumulation curves were con-
structed for each study area using EstimateS 9.1 (Colwell,
2013, 100 randomizations). In accordance with Unterseher
et al. (2008), first a non-parametric estimator was calculated
using the ‘default settings’ of EstimateS (Chao1, Chao et al.,
2005); second species accumulation curves were fitted with
the hyperbolic function y = ax/(b + x), with the parameter a
providing an estimate for species richness. Myxomycete
abundance was classified according to the ACOR scale of
Stephenson et al. (1993), based upon the proportion of a
species to the total number of records for each survey: R–rare (< 0.5%), O–occasional (> 0.5–1.5%), C–common
(> 1.5–3%), A–abundant (> 3%). Abundance-based datasets
from each of the eight study areas (see Appendix S2 in Sup-
porting Information) and environmental variables (geograph-
ical region and elevation, Table 1) were analysed in R (R
Core Team, 2015). Diversity between the geographical
regions (Neotropics versus Palaeotropics) and habitats (low-
land versus highland) was compared using the classical rich-
ness indices of Fisher’s alpha, the Shannon index (considers
richness and evenness) and the first three numbers of Hill’s
diversity series (Hill, 1973; Morris et al., 2014); differences
were tested for significance by a Wilcoxon test. In addition,
the most probable abundance distribution model was deter-
mined from rank-abundance plots (Whittaker, 1965) testing
five models following Wilson (1991): Null (fits the broken
stick model), Preemption (fits the geometric series or Moto-
mura model), log-Normal, Zipf and Mandelbrot. Both diver-
sity indices and distribution models were calculated in the
‘vegan’ package of R, using the functions renyi and radfit,
respectively. Community composition between geography
and elevation was examined using (1) clustering analysis and
non-metric multidimensional scaling (NMDS) based on Bray
Curtis distances and (2) the statistical test PERMANOVA
based on 999 permutations using the functions hclust,
metaMDS and adonis of R (see Appendix S3 for input files).
RESULTS
Basic data, sampling intensity and species
composition
Altogether, the surveys from eight areas (Table 1, see Fig. S3
in Appendix S1) included a total of 7585 myxomycete
records (2844 from Neotropical and 4741 from Asian
Palaeotropical forests). A total of 239 taxa (species and vari-
eties) were recorded. Neotropical forests were less diverse
(150 taxa) than Asian Palaeotropical forests (196 taxa, see
Appendix S2 for a collated list). This difference remained if
the rarefied values (based on the lower number of 2844
records) from an analysis of the species accumulation curves
were considered: 150.0 vs. 172.8 taxa.
On both continents, numerous taxa were represented by
only one record (singleton) for the entire region (Neotropics:
40 taxa, 27% of all taxa; Palaeotropics: 43 taxa, 22%). The
eight surveys were between 70% and 88% complete accord-
ing to the Chao1 estimator, and between 76% and 94%
according to a hyperbolic regression (Table 2, see Fig. S1 in
Appendix S1). If the degree of exhaustiveness was estimated
by a hyperbolic function y = ax/(b + x), the fit was better
(R = 0.885, a = 97.3, P < 0.0001) than for the final values of
the Chao1 estimator (R = 0.716, a = 94.3, P < 0.0001,
Fig. 2). Even for the South Luzon survey that had the highest
number of records, the survey was no more than 91%
(Chao1) and 94% (hyperbolic regression) complete. With
increasing sampling effort the number of singleton species
declined (linear regression y = ax + b for a scatter plot of
records per survey versus number of singleton species:
R = 0.676, a = �0.0077, P = 0.0066).
According to the ACOR scale, 72% of all taxa in the four
Neotropical surveys (pooled to a common species list, see
Appendix S2 and Fig S2 in Appendix S1) were rare, 17%
were occasional, 7% were common and 5% were abundant.
In spite of being represented by 1.7 times more records, 80%
of all taxa from the Asian Palaeotropical surveys were rare,
7% were occasional, 11% were common and only 3% were
abundant. The five most abundant species in the Neotropical
forest were Didymium iridis (211 records), Didymium
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Biogeographical assessment of myxomycete assemblages across the Tropics
squamulosum (194), Physarum compressum (190), the dwarf
form of Arcyria cinerea (172, described in Schnittler, 2000)
and Hemitrichia calyculata (119). In the Asian Palaeotropical
forests, the list was headed by Arcyria cinerea (933), Didy-
mium squamulosum (194), Perichaena depressa (155), Cri-
braria microcarpa (149) and Diderma hemisphaericum (144).
Non-metric multidimensional scaling ordinations display
contrasting signals of species turnover for geographical
(Neotropical versus Asian Palaeotropical) and elevational
(lowland versus highland) differences. Species composition
of Neotropical forests differed significantly from that of
Asian Palaeotropical forests (R2 = 0.278, P = 0.088); disper-
sion ellipses of the two assemblages in NMDS did not over-
lap (Fig. 3a). Cluster analysis using Bray Curtis dissimilarity
(Fig. 3c) confirmed this bipartition. In contrast, there is no
significant difference between lowland and highland sample
groups (Fig. 3b, R2 = 0.117, P = 0.474).
Species abundance distribution and diversity
The rank-abundance plots tested for different abundance dis-
tribution models showed comparable results for Neotropical
and Asian Palaeotropical forests. For datasets pooled for the
two different geographical regions, log-Normal was the best
fitting model; for the comparison of lowlands versus high-
lands the log-Normal model best fit for the former and Man-
delbrot model provided a slightly better fit for the latter
(Fig. 4). Boxplots for several estimators of species diversity
(Fig. 5) were not always higher for the Palaeotropics
(Fig. 5a), as would be expected from a comparison of species
richness. The trend for elevational differences is clearer, since
all five indices were higher for lowland than for highland for-
ests (Fig. 5b). However, none of these differences was signifi-
cant (comparison between lowland and highland areas, see
Table S1 of Appendix S1, P > 0.05; between Neotropical and
Table 2 Statistical analysis of individual-based species accumulation curves of myxomycetes for the eight regional surveys in the tropics
(giving the area by name and classified as L = lowland, H = highland), showing numbers of records (Rec), species (Sp), rarified species(SpR), and values for numbers of species to expect according to the Chao1 estimator (mean � SD) and a fit with a hyperbolic function
y = ax/(b + x), with a as the estimator for the number of species to be expected. The per cent values denote the proportion of speciesfound on the number of species expected.
SurveyFound Expected: Chao1 Expected: Hyperbolic
Area Rec Sp SpR Chao1 SD % a SD R %
NL: Guanacaste 441 80 80.0 104.9 13.0 76.2 101.2 0.3 0.999 79.0
NL: Yasuni 924 92 75.8 126.5 19.3 72.8 103.2 0.2 0.996 89.2
NH: Monteverde 522 76 71.2 108.3 16.0 70.2 99.7 0.4 0.997 76.3
NH: Maquipucuna 957 85 66.1 105.8 10.9 80.3 97.7 0.3 0.992 87.0
PL: South Luzon 2045 80 57.1 86.0 4.7 93.0 85.6 0.1 0.994 93.5
PL: Cat Tien 1105 105 81.2 120.3 8.3 87.3 120.4 0.2 0.996 87.2
PH: Chiang Mai 1147 133 96.4 151.2 8.4 88.0 162.5 0.3 0.997 81.8
PH: Bi Dup Nui Ba 444 74 73.8 94.0 10.5 78.8 100.2 0.3 0.998 73.8
Figure 2 Relationship between the number of records and exhaustiveness of a survey (number of myxomycete species found as
proportion of the number of species to expect) for eight tropical surveys according to the Chao1 estimator � SD (a) and a hyperbolicregression (b). The values for eight regional surveys were in turn fitted with a hyperbolic function y = ax/(b + x), indicated as a solid
line with 95% confidence intervals as dotted lines. This fit results in estimates of the maximum exhaustiveness for an infinite number ofrecords of 94.2% (Chao1, R = 0.716) and 97.3% (hyperbolic regression, R = 0.885).
Journal of Biogeography 44, 1524–1536ª 2017 John Wiley & Sons Ltd
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N. H. A. Dagamac et al.
Asian Palaeotropical forests, P > 0.05). Similarly, species
richness was not higher in lowland forests, since rarefied
means were 73.5 � 11.2 for lowland and 76.9 � 13.4 for
highland areas (rarefied figures based on the lowest number
of 441 records for a survey, Table 2). This was caused by the
very high taxon number for one highland survey (northern
Thailand, 133 taxa, rarefied value 96.4).
DISCUSSION
Differences in species abundances and composition
between the Neotropics and Asian Palaeotropics
In recent years, abundance-based myxomycete data from the
Asian Palaeotropics have become available, allowing a com-
parison with Neotropical inventories. Almost all myxomycete
surveys revealed a high proportion of rare taxa, often found
only once in an area (e.g. Schnittler et al., 2002). To com-
pensate for the random component introduced by the rather
high proportion of rare species (between 15% and 38% of all
species in our surveys were represented by single records) we
considered only surveys recording species abundances. Four
pairs of large datasets were compiled to test the prima facie
null hypothesis that neither diversity nor species composition
differs between Neotropical and Asian Palaeotropical forests.
Given that similar macroecological conditions exist between
regions, this can be expected if there is efficient long-distance
dispersal by spores.
For a regional survey, there was some degree of hetero-
geneity in targeted microhabitats and/or substrata. Even for
large datasets, such as that from South Luzon, the number of
species recorded was lower than the number of expected spe-
cies. This was predicted to be the case even for infinitely
large surveys, as indicated by final percentages of 92% (esti-
mated via analysis of species accumulation curves based on
the Chao1 estimator) and 97% (hyperbolic regression, Fig. 2)
and a higher sampling effort seems to reduce the proportion
of rare species for a survey. These results reflected the
unavoidable degree of heterogeneity for surveys covering a
larger area. Nevertheless, the species accumulation curves
generated for the eight study areas suggest that the sampling
effort was sufficient to recover most of the species that are
realistically possible to recover.
Asian Palaeotropic forests seemed to be richer in species of
myxomycetes than Neotropic forests (rarefied species num-
bers: 172.8 vs. 150.0). The presence of conifers (Pinus spp.)
with acidic bark and wood in the mountains of Vietnam (Bi
Dup Nui Ba) and Thailand (Chiang Mai) may contribute,
Figure 3 Non-metric multidimensional scaling (NMDS) of species occurrences for the eight surveys based on (a) geographic location and(b) elevational location. Black dots represent the position of myxomycete species in the ordination space. Coloured circles and squares
represent the regions/areas; coloured ellipses denote dispersion based on standard deviation of point scores. (c) Clustering analysis using BrayCurtis dissimilarity distance based on species composition (species and abundances). [Colour figure can be viewed at wileyonlinelibrary.com]
Journal of Biogeography 44, 1524–1536ª 2017 John Wiley & Sons Ltd
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Biogeographical assessment of myxomycete assemblages across the Tropics
since here several myxomycete taxa (Barbeyella minutissima
Meyl., Echinostelium brooksii Whitney, E. colliculosum Whitney
& Keller, Lamproderma columbinum (Pers.) Rostaf., Licea
kleistobolus Martin, Lindbladia tubulina Fr., Paradiacheopsis
rigida (Brandza) Nann.-Bremek., and Trichia persimilis Karst.)
were recorded that are known to be common in coniferous
forests in temperate zones. Neotropical highland regions
investigated in this study lack conifers, but these do occur,
together with some of the species of myxomycete mentioned
above, on the summits of Mexican volcanoes (Lado & Wrigley
de Basanta, 2008). In addition, northern Thailand (Chiang
Mai) yielded the highest number of species (133), and this was
the only dataset compiled from several researchers working
independently. For this area, we cannot avoid the possibility
that in a few cases a particular taxon was assigned to two dif-
ferent names, causing overestimation of species numbers. The
dataset from northern Thailand also contained the highest
proportion of rare species (69.2%); and the number of single-
ton species (33) was above average (23.5).
The higher species richness of Asian Palaeotropical forests
was not reflected by all of the computed diversity indices,
but all indices were consistently higher for lowland than for
highland forests (Fig. 5b). These differences were not
statistically significant (Wilcoxon test) but were in congru-
ence with observations that myxomycete diversity in tropical
forests decreases with increasing elevation (Schnittler &
Stephenson, 2000; Stephenson et al., 2004b; Rojas &
Stephenson, 2008). In constantly wet highland forests, myx-
omycetes seemed to utilize aerial litter, which dries out fas-
ter, more often than ground microhabitats (Schnittler &
Stephenson, 2000; Lado et al., 2003, 2017). Therefore, the
moisture regime, not elevation per se may be the driver of
differences in the abundance of fruiting bodies (Rojas et al.,
2016).
Interestingly, when we consider species composition, a
statistically significant difference was observed among myx-
omycete assemblages in relation to geography (Neotropics
versus Palaeotropics) but not in relation to habitat type
(lowland versus highland forests). As in fungal endophytes
(Langenfeld et al., 2013), soil protist assemblages (Foissner,
2007; Bates et al., 2013), and marine ciliates (Stock et al.,
2013), geographical location best explains the differences in
assemblage composition. A biogeographical study of myx-
omycetes that focused only on tropical highland forests
found a similar pattern: a cluster analysis separated myx-
omycete assemblages recorded from Thailand from those of
Figure 4 Rank abundance plots based onthe abundance of species for the (a, b)
geographical (Neotropics versusPalaeotropic) and (c, d) elevational
(Lowland versus Highland) gradient fittedwith five species distribution models. All
records from region or elevation (foursurveys each) were pooled. The model
showing the best fit is highlighted by a thickline. [Colour figure can be viewed at
wileyonlinelibrary.com]
Journal of Biogeography 44, 1524–1536ª 2017 John Wiley & Sons Ltd
1530
N. H. A. Dagamac et al.
Figure 5 Box plot showing the comparison of five different diversity indices (Alpha = Fisher’s alpha; Shannon = Shannon’s H index;
N0 = species richness; N1 = exponent of Shannon diversity and N2 = inverse of Simpson) in relations to (a) geography and (b)elevation. Data from four study areas were pooled according to (a) geography (Neo- versus Palaeotropics) and (b) elevation (lowland
versus highland regions).
Journal of Biogeography 44, 1524–1536ª 2017 John Wiley & Sons Ltd
1531
Biogeographical assessment of myxomycete assemblages across the Tropics
the Americas (Rojas et al., 2012b). Although elevation deter-
mined habitat availability (Rojas et al., 2010; Dagamac et al.,
2014) and forest types (Novozhilov et al., 2000; Rojas et al.,
2011), the high overlap of species composition between
assemblages of lowland and highland areas showed that
myxomycetes seem to find in both elevations suitable
microhabitats for fruiting.
Are there myxomycetes restricted to the tropics?
Several species were found in a single survey or a pair of
surveys only. Comatricha spinispora Novozh. & Mitchell (26
records), Diderma pseudostestaceum Novozh. & Mitchell
(14), D. cattiense Novozh. & Mitchell (18) and Perichaena
echinolophospora Novozh. & Stephenson (4) were found only
in surveys conducted in Vietnam. Craterium paraguayense
(Speg.) G. Lister (4) and Lamproderma muscorum (Lev.)
Hagelst. (7) were reported exclusively from the Costa Rican
highlands (Monteverde) dataset and Diachea silvaepluvialis
Farr (6) was found exclusively in Ecuador (Yasuni). More
species were found exclusively in either the Neotropical (35)
or the Asian Palaeotropical region (68), of which 24 and 30
species, respectively, were singletons. For instance, Cera-
tiomyxa morchella Welden (45 records) and C. sphaeros-
perma Boedijn (24) were found only in the Neotropical
region; Physarum echinosporum Lister (55) and Cribraria
minutissima Schwein. (41) occurred exclusively in surveys
from the Asian Palaeotropical region. However, at this
point, we have to consider the low taxonomic resolution
provided by a morphological-based approach. All studies
that entered the ‘biospecies’ level via cultivation and com-
patibility experiments (Clark & Haskins, 2013) or via molec-
ular markers (Feng & Schnittler, 2015) found that a given
‘morphospecies’ comprised several putative biospecies (de-
fined as reproductively isolated units). A first local survey
based on fructifications with a full barcoding component
estimated the relationship between morphospecies and ribo-
types, the latter indicating the existence of different biospe-
cies, to be 1:2–10 (Feng & Schnittler, 2017). Therefore, a
cosmopolitan morphospecies such as Arcyria cinerea (Bull.)
Pers., is likely to consist of several biospecies (Clark et al.,
2002) if studied by molecular methods, and therefore puta-
tive biospecies may be more restricted in distribution. This
is not obvious when looking at distribution ranges of myx-
omycetes (see examples in Stephenson et al., 2008) since
many morphospecies appear to have large or even cos-
mopolitan ranges. In other words, as in the case of pyreno-
mycetous fungi (Vasilyeva & Stephenson, 2014), we should
expect at least some species to be restricted to certain
regions of the world.
Morphological-based surveys support moderate
endemicity for eukaryotic protist
Given the apparent rarity of fructifications for many myx-
omycetes (Stephenson, 2011), abundance data are important
to identify cases of moderate endemicity. Ceratiomyxa morch-
ella Welden (Neotropics) and Physarum echinosporum Lister
(Asian Palaeotropics) may be good examples, both represent-
ing unmistakable morphospecies that were common only in
one of the two regions. For this finding, we can assume that
despite intense surveys in similar tropical environments, geo-
graphical barriers between continents have played a role in
the apparent differences noted for species abundance and
composition. We can also expect that geographical differ-
ences found in this study will become more evident if large
datasets on molecular diversity become available for myx-
omycetes. In a related morphological-based approach,
Estrada-Torres et al. (2013) considered numerous environ-
mental factors and found that historical geography explained
best the distribution of myxomycete assemblages in the
Americas. Even if this study used presence/absence data only,
they similarly noted that some species (e.g. Diderma tehuaca-
nense Estrada, D. Wrigley & Lado and Perichaena stipitata
Lado, Estrada & D.Wrigley) were found exclusively in one
area.
In summary, biogeographic patterns of myxomycetes in
the tropics provided evidence that species composition is dif-
ferent and this is due to at least some morphologically recog-
nizable taxa that are indeed restricted to particular
geographical areas, some appeared to be regionally or locally
endemic, and thus we may expect moderate endemicity to be
the rule rather than the exception.
ACKNOWLEDGEMENTS
N.H.A.D. acknowledges the German Academic Exchange
Service (DAAD) for a PhD scholarship. We are grateful to
Eva Heinrich, Melissa Pecundo, Arturo Estrada-Torres and
Diana Wrigley de Basanta for technical assistance with field
collecting and species determination. Y.K.N. was supported
by the scientific programs ‘Ecolan-1.2’ of the Russian-Viet-
namese Tropical Scientific and Technological Centre (Viet-
nam, Ho Chi Minh City) and a grant ‘Mycobiota of
southern Vietnam’, 01201255603 (Russia, St. Petersburg)
and is grateful to Ludmila A. Kartzeva (The Core Facility
Center ‘Cell and Molecular Technologies in Plant Science’
at the Komarov Botanical Institute RAS, St. Petersburg,
Russia) for the technical support (SEM). Surveys in the
Neotropics were enabled by several grants (DEB-9705464,
DEB-0102895 and DEB-0316284) from the National Science
Foundation and one grant (8890-11) from the National
Geographic Society to S.L.S. C.L. was funded by the US-
Spain Science and Technology Fulbright Cooperation Pro-
gram (Ref. 99075), and by the grant (CGL2014-52584P)
from the Spanish Government (Myxotropic project). C.R.
has been supported by University of Costa Rica through
research codes 731-B4-072 and 731-B5-062. T.E.D.C. was
supported by the Research Center for Natural and Applied
Sciences of University of Santo Tomas. M.U. acknowledges
financial support from the DAAD for his collection trip to
Thailand.
Journal of Biogeography 44, 1524–1536ª 2017 John Wiley & Sons Ltd
1532
N. H. A. Dagamac et al.
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SUPPORTING INFORMATION
Additional Supporting Information may be found in the
online version of this article:
Appendix S1 Supplementary figures and tables.
Appendix S2 Collated database of the study areas.
Appendix S3 Input files used in R.
BIOSKETCH
Nikki Heherson A. Dagamac is broadly interested in bio-
geography and biodiversity of tropical myxomycetes. The
group worked for a number of decades on developing a bet-
ter understanding of the global distribution patterns, taxon-
omy and ecology of myxomycetes.
Author contributions: M.S. conceptualized and designed the
present study; data from the Neotropical region were taken
from surveys of M.S., Y.K.N., C.L., C.R. and S.L.S; data from
the Palaeotropical region originated from field surveys of
N.H.A.D., Y.K.N., T.E.D.C., M.U. and M.S; N.H.A.D. com-
piled all data from the eight surveys, assembled the initial spe-
cies lists and collated the dataset; N.H.A.D., M.U. and M.S.
performed the ecological analysis of the dataset and interpreted
the results; N.H.A.D. and M.S. prepared the manuscript, which
was approved by all authors and improved by Y.K.N., C.L. and
C.R. S.L.S. did the English correction of the text.
Editor: Len N. Gillman
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